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hal.structure.identifierBiodiversité, Gènes & Communautés [BioGeCo]
dc.contributor.authorVITASSE, Yann
hal.structure.identifierBiodiversité, Gènes & Communautés [BioGeCo]
dc.contributor.authorDELZON, Sylvain
hal.structure.identifierEcologie Systématique et Evolution [ESE]
hal.structure.identifierAgroParisTech
dc.contributor.authorDUFRENE, Eric
hal.structure.identifierEcologie Systématique et Evolution [ESE]
hal.structure.identifierAgroParisTech
dc.contributor.authorPONTAILLER, Jean-Yves
hal.structure.identifierBiodiversité, Gènes & Communautés [BioGeCo]
dc.contributor.authorLOUVET, Jean-Marc
hal.structure.identifierBiodiversité, Gènes & Communautés [BioGeCo]
dc.contributor.authorKREMER, Antoine
hal.structure.identifierBiodiversité, Gènes & Communautés [BioGeCo]
dc.contributor.authorMICHALET, Richard
dc.date.issued2009
dc.identifier.issn0168-1923
dc.description.abstractEnConsequences of climate warming on tree phenology are readily observable, but little is known about the differences in phenological sensitivity to temperature between species and between populations within a species. The aim of the present study is to compare phenological sensitivities to temperature of seven woody species between each other and within-species between two geographical areas using both altitudinal and temporal gradients (Abies alba, Acer pseudoplatanus, Carpinus betulus, Fagus sylvatica, Fraxinus excelsior, Ilex aquifolium and Quercus petraea). The timing of leaf unfolding was monitored (i) over 2 years along two altitudinal gradients in the Pyrénées mountains (six species), and (ii) over 22 years in Fontainebleau forest (four species). Three species were present in both areas which allowed us to compare their phenological sensitivity to temperature over altitudinal and temporal gradients. Along altitudinal gradients, we observed for all species an advance in leaf unfolding with decreasing elevation, ranging from 11 to 34 days 1000 m−1 for beech and oak, respectively. Across the temporal gradient, we found significant advances in leaf unfolding for oak (−0.42 days year−1) and ash (−0.78 days year−1) since 1976, whereas no significant advance was observed for beech and hornbeam. For both gradients and for all species, significant correlations were found between leaf unfolding dates and temperature, except for beech in the temporal study. Moreover, we highlighted that phenological sensitivity to temperature was very similar between the two geographically separated populations (Pyrénées and Fontainebleau forests). Thus, oak had the strongest sensitivity (−7.48 and −7.26 days °C−1 in altitudinal and temporal gradient, respectively) and beech had the lowest (−2.09 and −2.03 days °C−1). Our results suggest that population sensitivity to global warming might be stable for a given species, in spite of its possible local adaptation.
dc.language.isoen
dc.publisherElsevier Masson
dc.subjectCHARME
dc.subjectDIVERSITÉ DE POPULATION
dc.subject.enLEAF UNFOLDING
dc.subject.enALTITUDINAL GRADIENT
dc.subject.enCLIMATE CHANGE
dc.subject.enTEMPERATE FORESTS
dc.subject.enTREE POPULATIONS
dc.subject.enCHENE
dc.subject.enHETRE
dc.title.enLeaf phenology sensitivity to temperature in European trees: Do within-species populations exhibit similar responses?
dc.typeArticle de revue
dc.identifier.doi10.1016/j.agrformet.2008.10.019
dc.subject.halSciences du Vivant [q-bio]/Sciences agricoles/Sylviculture, foresterie
bordeaux.journalAgricultural and Forest Meteorology
bordeaux.page735-744
bordeaux.volume149
bordeaux.issue5
bordeaux.peerReviewedoui
hal.identifierhal-02668790
hal.version1
hal.popularnon
hal.audienceInternationale
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-02668790v1
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